Abstract
Differences in shape between Plinian eruption columns and lateral blast flows on Earth and between umbrella-shaped and diffuse plumes on Jupiter's moon, Io, are discussed in terms of a generalized model for thermodynamic properties and geometry of a volcanic system. -R.A.H. US Geological Survey, Flagstaff, AZ, USA.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 143-157 |
| Number of pages | 15 |
| Journal | Unknown Journal |
| State | Published - 1984 |
| Externally published | Yes |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences